Session Objectives
Session 8: Physical Meteorology and Visibility
Upon completion of this session, a participant should be able to
do the following:
- List two general differences between aerosol concentrations
over oceans and aerosol concentrations over continents.
- Compare and contrast Rayleigh and Mie scattering of visible
light. Determine which form of scattering is occurring in a given
scenario.
- Explain how it is possible for air to have a relative
humidity greater than 100% and state the range of typical
supersaturations that are observed in our atmosphere.
- State the major function of aerosols in cloud formation.
- State the two growth processes a liquid water droplet will
experience as it grows from initial formation to the size of a
typical raindrop.
- Describe how the curvature effect and the solution effect
work in opposition to each other during droplet growth by
diffusion.
- List several phenomena which result from high concentrations
of aerosols in the atmosphere and frequently reduce visual air
quality.
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